Provenance of the detrital garnets and spinels from the Albian sediments of the Czorsztyn Unit (Pieniny Klippen Belt, Western Carpathians, Slovakia)

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Provenance of the detrital garnets and spinels from the Albian sediments of the Czorsztyn Unit (Pieniny Klippen Belt, Western Carpathians, Slovakia)

According to earlier concepts, the Czorsztyn Unit (Oravic Superunit, Pieniny Klippen Belt, Western Carpathians) sedimented on the isolated Czorsztyn Swell which existed in the Middle Jurassic-Late Cretaceous time in the realm of the Outer Western Carpathians. This paper brings new data providing an alternative interpretation of its Cretaceous evolution. They are based on heavy mineral analysis of the Upper Aptian/Lower Albian sediments of the Czorsztyn Unit. They rest upon a karstified surface after a Hauterivian-Aptian emersion and are represented by condensed, red marly organodetritic limestones with some terrigenous admixture (Chmielowa Formation). The heavy mineral spectrum is dominated by spinels, followed by garnet, with lesser amounts of zircon, rutile and tourmaline. The composition of the majority of the detrital garnets shows that they were derived from primary HP/UHP parental rocks which were recrystallized under granulite and amphibolite facies conditions. The garnets were most probably derived directly from the magmatic and metamorphic rocks of the Oravic basement, as the high-pyrope garnets are known to be abundant in Mesozoic sediments all over the Outer Western Carpathians. The presence of spinels is surprising. According to their chemistry, they were mostly derived from mid-oceanic ridge basalts (MORB) peridotites, supra-subduction zone peridotites (harzburgites) and transitional lherzolite/harzburgite types. Only a lesser amount of spinels was derived from volcanics of BABB composition (back-arc basin basalts). The presence of this ophiolitic detritus in the Czorsztyn Unit is difficult to explain. Ophiolitic detritus appeared in the Aptian/Albian time only in the units which were considered to be more distant, because they were situated at the boundary between the Central and the Outer Western Carpathians (Klape Unit, Tatric and Fatric domains). The hypothetical Exotic Ridge which represented an accretionary wedge in front of the overriding Western Carpathian internides was considered to be a source of the clastics. In previous paleogeographical reconstructions, the Czorsztyn Unit was situated north of the Pieniny Trough (considered to be one of the branches of the Penninic-Vahic Ocean). In the trough itself, the ophiolitic detritus appeared as late as in the Senonian and there was no way it could reach the Czorsztyn Swell which was considered to be an isolated elevation. The new results presented herein show that these reconstructions do not fit the obtained data and infer a possibility that the Czorsztyn sedimentary area was not isolated in the Cretaceous time and it was situated closer to the Central Carpathian units than previously thought. A new paleogeographical model of the evolution of the Pieniny Klippen Belt is presented in the paper: Oravic segment was derived from the Moldanubian Zone of the Bohemian Massif by the Middle Jurassic rifting which caused block tilting where most of the Oravic units were arranged north of the Czorsztyn Swell. The Oravic segment was situated in the lateral continuation of the Central and Inner Western Carpathians from which it was detached by later clockwise rotation. The Oravic segment was then laterally shifted in front of the Central Western Carpathians, together with remnants of the Meliatic suture zone which represented a source for the exotics to the Klape, Tatric, Fatric and Oravic units.

Andrusov D. 1938: Geological research of the Inner Klippen Belt, Western Carpathians. Part III (Tectonics). Rozpr. St. Geol. Úst. ČSR 9, 1-135 (in Czech and French).

Andrusov D. 1945: Geological research of the Inner Klippen Belt, Western Carpathians. Part IV (Stratigraphy of the Dogger and Malm), Part V (Stratigraphy of the Cretaceous). Práce Štát. Geol. Úst. 13, 1-176 (in Slovak).

Aubrecht R. 1993: Clastic admixture in Dogger crinoidal limestones of Czorsztyn Unit. Geol. Carpathica 44, 105-111.

Aubrecht R. 2001: Jurassic heavy mineral distribution provinces of the Western Carpathians. Miner. Slovaca 33, 473-486.

Aubrecht R. & Méres Š. 1999: Possible Moldanubic provenance of the Pieniny Klippen Belt crystalline basement deduced from detrital garnets. Geol. Carpathica, Spec. Issue 50, 13-14.

Aubrecht R. & Méres Š. 2000: Exotic detrital almandine-pyrope garnets in the Jurassic sediments of the Pieniny Klippen Belt and Tatric Zone: where did they come from? Miner. Slovaca 32, 17-28.

Aubrecht R. & Túnyi I. 2001: Original orientation of neptunian dykes in the Pieniny Klippen Belt (Western Carpahtians): the first results. Contr. Geophys. Geodes. 31, 3, 557-578.

Aubrecht R., Krobicki M., Sýkora M., Mišík M., Boorová D., Schlögl J., Šamajová E. & Golonka J. 2006: Early Cretaceous hiatus in the Czorsztyn Succession (Pieniny Klippen Belt, Western Carpathians): submarine erosion or emersion? Ann. Soc. Geol. Pol. 76, 161-196.

Aubrecht R., Méres Š., Gradziński M. & Sýkora M. 2007: Provenance of detritic garnets in the Middle Jurassic clastic sediments of the Cracow Region. Miner. Pol., Spec. Pap. 31, 47-52.

Árgyelán B. G. 1992: Chemical investigations of detrital chromian spinels of Cretaceous clastic formations of the Gerecse Mountains, Hungary. Terra Abstr. 4, Suppl. 2, p. 3.

Árgyelán B. G. 1996: Geochemical investigations of detrital chrome spinels as a tool to detect an ophiolitic source area (Gerecse Mts. Hungary). Acta Geol. Hung. 39, 341-368.

Árgyelán G. & Császár G. 1998: Detrital chrome spinels in Jurassic formations of the Gerecse Mountains. Földt. Közl. 128, 321-360.

Began A., Borza K., Salaj J. & Samueal O. 1965: On the age of the Upohlava Conglomerates. Geol. Práce, Spr. 36, 123-138.

Birkenmajer K. 1977: Jurassic and Cretaceous lithostratigraphic units of the Pieniny Klipen Belt, Carpathians, Poland. Stud. Geol. Pol. 45, 1-158.

Birkenmajer K. 1987: The Trawne Member (Upper Albian-Upper Cenomanian) — a flysch development in the Branisko Nappe, Pieniny Klippen Belt, Carpathians. Stud. Geol. Pol. 92, 29-40.

Birkenmajer K. 1988: Exotic Andrusov Ridge: its role in plate-tectonic evolution of the West Carpathian foldbelt. Stud. Geol. Pol. 91, 7-92.

Birkenmajer K. & Pécskay Z. 2000: Early Cretaceous K-Ar age of a large basalt olistolith at Biala Woda, Pieniny Klippen Belt, West Carpathians, Poland. Stud. Geol. Pol. 117, 27-35.

Birkenmajer K., Kozur H. & Mock R. 1990: Exotic Triassic pelagic limestone pebbles from the Pieniny Klippen Belt of Poland: a further evidence for early Mesozoic rifting in West Carpathians. Ann. Soc. Geol. Pol. 60, 3-44.

Császár G. & Árgyelán B. G. 1994: Stratigraphical and micromineralogical investigation of Lower Cretaceous sediments in Gerecse Mts. Hungary. Cretaceous Research 15, 417-434.

Csontos L. & Vörös A. 2004: Mesozoic plate tectonic reconstruction of the Carpathian region. Palaeogeogr. Palaeoclimatol. Palaeoecol. 210, 1-56.

Čopjaková R., Sulovský P. & Otava J. 2001: Utilization of detrital garnet chemistry for determination of the provenance and lithostratigraphy of the Culm of Drahany Upland. Miner. Slovaca 33, 5, 509-511 (in Czech).

Čopjaková R., Sulovský P. & Paterson B. A. 2005: Major and trace elements in pyrope-almandine garnets as sediment provenance indicators of the Lower Carboniferous Culm sediments, Drahany Uplands, Bohemian Massif. Lithos 82, 51-70.

Dal Piaz G. V., Martin S., Villa I. M., Cosso G. & Marschalko R. 1995: Late Jurassic blueschist facies pebbles from the Western Carpathian orogenic wedge and paleostructural implications for Western Tethys evolution. Tectonics 14, 874-885.

Decker K., Faupl P. & Müller A. 1987: Synorogenic sedimentation on the Northern Calcareous Alps during the Early Cretaceous. In: Flügel H. W. & Faupl P. (Eds.): Geodynamics of the Eastern Alps. Deuticke, Wien, 126-141.

Deer W. A., Howie R. A. & Zussman J. 1992: An introduction to the rock-forming minerals (2nd Edition). Longman, England, 1-696.

Dick H. J. B. & Bullen T. 1984: Chromian spinel as a petrogenetic indicator in abyssal and Alpine-type peridotites and spatially associated lavas. Contr. Mineral. Petrology 86, 54-76.

Eynatten H. V. & Gaupp R. 1999: Provenance of Cretaceous synorogenic sandstones in the Eastern Alps: constraints from framework petrography, heavy mineral analysis and mineral chemistry. Sed. Geol. 124, 81-111.

Faryad S. W. & Vozárová A. 1997: Geology and metamorphism of the Zemplinicum basement unit (Western Carpathians). In: Grecula P., Hovorka D. & Putiš M. (Eds.): Geological evolution of the Western Carpathians. Mineralia Slovaca-Monograph, Bratislava, 351-358.

Faryad S. W., Ivan P. & Jacko S. 2005: Metamorphic petrology of metabasites from the Branisko and Čierna hora Mountains (Western Carpathians Slovakia). Geol. Carpathica 56, 3-16.

Faupl P. & Pober E. 1991: Zur Bedeutung detritischer Cromspinelle in den Ostalpen: Ophiolitischer Detritus aus der Vardarsutur. In: Lobitzer H. & Császár G. (Eds.): Jubiläumsschrift 20 Jahre Geologische Zusammenarbeit Ősterreich-Ungarn. Teil 1, Geologische Bundesanstalt, Wien, 133-143.

Faupl P. & Wagreich M. 1992: Cretaceous flysch and pelagic sequences of the Eastern Alps: Correlations, heavy minerals, and palaeogeographical implications. Cretaceous Research 13, 387-403.

Grzebyk J. & Leszczyński S. 2006: New data on heavy minerals from the Upper Cretaceous-Paleogene flysch of the Beskid Śląski Mts. (Polish Carpathians). Geol. Quart. 50, 265-280.

Hartley A. J. & Otava J. 2001: Sediment provenance in a deep marine foreland basin: the Lower Carboniferous Culm Basin, Czech Republic. J. Geol. Soc. London 158, 137-150.

Havlena V. 1956: Plant spores from Carboniferous pebbles of cannel coal from the Carpathian Cretaceous. Čas. Min. Geol. 1, 344-351 (in Czech with English summary).

Hollister L. S. 1966: Garnet zoning: an interpretation based on the Rayleigh fractionation model. Science 154, 1647-1651.

Hovorka D. & Méres Š. 1990: Clinopyroxene-garnet metabasites from the Tribeč Mts. (Central Slovakia). Miner. Slovaca 22, 533-538 (in Slovak with English summary).

Hovorka D. & Méres Š. 1991: Pre-Upper Carboniferous gneisses of the Strážovské vrchy Upland and the Malá Fatra Mts. (the Western Carpathians). Acta Geol. Geogr. Univ. Com., Geol. 46, 103-169.

Hovorka D. & Spišiak J. 1997: Medium-grade metamorphics of the Gemeric unit (central Western Carpathians). In: Grecula P., Hovorka D. & Putiš M. (Eds.): Geological evolution of the Western Carpathians. Mineralia Slovaca—Monograph, Bratislava, 315-332.

Hovorka D., Méres Š. & Caňo F. 1992: Petrology of the garnet clinopyroxene metabasites from the Malá Fatra Mts. Miner. Slovaca 24, 45-52 (in Slovak with English summary).

Hovorka D., Méres Š. & Krištín J. 1987: Garnets from paragneisses of the central zone of the West Carpathians. Miner. Slovaca 19, 4, 289-309.

Jablonský J. 1978: Contribution to the knowledge of the Zliechov Series Albian in the Strážovské vrchy Mts. In: Vozár J. (Ed.): Paleogeographic development of the Western Carpathians. GÚDŠ, Bratislava, 175-188 (in Slovak).

Jablonský J. 1986: Sedimentological study of the Poruba Formation (Albian-Cenomanian) of the Tatric and Zliechov sequences. Unpubl. PhD. Thesis: Comenius University, Bratislava, 1-211 (in Slovak).

Jablonský J. 1992: Rossfeld Formation in Krížna and Choč nappes, Western Carpathians. Terra Abstr. 4, Suppl. 2, p. 37.

Jablonský J., Sýkora M. & Aubrecht R. 2001: Detritic Cr-spinels in Mesozoic sedimentary rocks of the Western Carpathians (overview of the latest knowledge). Miner. Slovaca 33, 487-498 (in Slovak with English summary).

Janák M. & Lupták B. 1997: Pressure-temperature conditions of high grade metamorphism and migmatitization in the Malá Fatra crystalline complex, the Western Carpathians. Geol. Carpathica 48, 5, 287-302.

Janák M., O'Brien P. J., Hurai V. & Reutel Ch. 1996: Metamorphic evolution and fluid composition of garnet-clinopyroxene amphibolites from the Tatra Mts., Western Carpathians. Lithos 39, 57-79.

Janák M., Plašienka D., Frey M., Cosca M., Schmidt S. T., Lupták B. & Méres Š. 2001: Cretaceous evolution of a metamorphic core complex, the Veporic unit, Western Carpathians (Slovakia): P-T conditions and in situ 40Ar/39Ar UV laser probe dating of metapelites. J. Metamorph. Geology 19, 197-216.

Janák M., Méres Š. & Ivan P. 2007: Petrology and metamorphic P-T conditions of eclogites from northern Veporic Unit (Western Carpathians, Slovakia). Geol. Carpathica 58, 2, 121-131.

Janoušek V., Gerdes A., Vrána S., Finger F., Erban V., Friedl G. & Braithwaite C. J. R. 2006: Low-pressure granulites of the Lišov Massif, Southern Bohemia: Viseán metamorphism of Late Devonian plutonic arc rocks. J. Petrology 47, 4, 705-744.

Janoušek V., Krenn E., Finger F., Míková J. & Frýda J. 2007: Hyperpotassic granulites from the Blanský les Massif (Moldanubian Zone, Bohemian Massif) revisited. J. Geosci. 52, 73-112.

Kamenetsky V. S., Crawford A. J. & Meffre S. 2001: Factors controlling chemistry of magmatic spinel: an empirical study of associated olivine, Cr-spinel and melt inclusion from primitive rocks. J. Petrology 42, 655-671.

Korikovsky S. P., Dupej J., Boronikhin V. A. & Zinovieva N. G. 1990: Zoned garnets and their equilibria in mica schists and gneisses of Kohút crystalline complex, Hnúšťa region, Western Carpathians. Geol. Zbor. Geol. Carpath. 41, 99-124.

Kretz R. 1983: Symbols for rock forming minerals. Amer. Mineralogist 68, 277-279.

Krogh Ravna E. J. & Terry M. P. 2004: Geothermobarometry of UHP and HP eclogites and schists — an evaluation of equilibria among garnet-clinopyroxene-kyanite-phengite-coesite/quartz. J. Metamorph. Geology 22, 579-592.

Kryza R., Pin C. & Vielzeuf D. 1996: High-pressure granulites from the Sudetes (south-west Poland): evidence of crustal subduction and collisional thickening in the Variscan Belt. J. Metamorph. Geology 14, 531-546.

Lenaz D., Kamenetsky V. S., Crawford A. J. & Princivalle F. 2000: Melt inclusion in detrital spinel from the SE Alps (Italy-Slovenia): a new approach to provenance studies of sedimentary basins. Contr. Mineral. Petrology 139, 748-758.

Lexa J., Bezák V., Elečko M., Eliáš M., Konečný V., Less Gy., Mandl G. W., Mello J., Pálenský P., Pelikán P., Polák M., Potfaj M., Radócz Gy., Ryłko W., Schnabel G. W., Stráník Z., Vass D., Vozár J., Zelenka T., Biely A., Császár G., Čtyroký P., Kaličiak M., Kohút M., Kovács S., Mackiv B., Maglay J., Nemčok J.†, Nowotny A., Pentelényi L., Rakús M. & Vozárová A. 2000: Geological map of Western Carpathians and adjacent areas, 1:500,000. Ministry of the Environment of Slovak Republic, Geological Survey of Slovak Republic, Bratislava.

Łoziński J. 1959: Heavy minerals of the Lower and Middle Cretaceous sandstones in the Pieniny Klippen Belt. Ann. Soc. Geol. Pol. 29, 119-125.

Maheľ M. 1981: Penninic units in the Western Carpathians from the point of view of global tectonics. Miner. Slovaca 13, 289-306 (in Slovak with English summary).

Maheľ M. 1989: Pieniny Klippen Belt from the geodynamic model aspect. Miner. Slovaca 21, 99-108 (in Slovak with English summary).

Marschalko R. 1986: Evolution and geotectonic consequence of the Cretaceous flysch of the Pieniny Klippen Belt. Publ. Veda, Bratislava, 1-137 (in Slovak with Russian and English summaries).

Marschalko R. & Rakús M. 1997: Development of the Cretaceous flysch in the Klape unit and the recyclicity problem of the clastic material. In: Plašienka D., Hók J., Vozár J. & Elečko M. (Eds.): Alpine evolution of the Western Carpathians and related areas. Internat. Conf., Sept. 1997, Introduct. articles to the excursion, GS SR, D. Štúr Publ., Bratislava, 71-78.

Massonne H. J. & Bautsch H. J. 2004: Ultrahigh and high pressure rocks of Saxony. In: 32nd IGC, Florence-Italy, August 20-28, 2004, Field Trip Guide Book — B21, 2, 1-36.

Matějka A. & Andrusov D. 1931: Aperçu de la géologie des Carpathes occidentales de la Slovaquie centrale et les régions avoisinants. Knih. St. Geol. Úst. ČSR 13A, 19-163.

Medaris L. G. Jr., Beard B. L., Johnson C. M., Valley J. W., Spicuzza M. J., Jelínek E. & Mísař Z. 1995a: Garnet pyroxenite and eclogite in the Bohemian Massif: Geochemical evidence for Variscan recycling of subducted lithosphere. Geol. Rdsch. 84, 489-505.

Medaris L. G. Jr., Jelínek E. & Mísař Z. 1995b: Czech eclogites: Terrane settings and implications for Variscan tectonic evolution of the Bohemian Massif. Eur. J. Mineral. 7, 7-78.

Medaris L. G., Fournelle J. H., Ghent E. D., Jelínek E. & Mísař Z. 1998: Prograde eclogites in the Gföhl Nappe, Czech Republic: new evidence on Variscan high-pressure metamorphism. J. Metamorph. Geology 16, 563-576.

Medaris L. G. Jr., Wang H., Jelínek E., Mihaljevič M. & Jakeš P. 2005: Characteristics and origins of diverse Variscan peridotites in the Gföhl nappe, Bohemian Massif, Czech Republic. Lithos 82, 1-23.

Medaris L. G., Beard B. L. & Jelínek E. 2006a: Mantle-derived, UHP garnet pyroxenite and eclogite in the Moldanubian Gföhl Nappe, Bohemian Massif: A geochemical review, new P-T determinations, and tectonic interpretation. Int. Geol. Rev. 48, 765-777.

Medaris L. G. Jr., Ghent E. D., Wang H. F., Fournelle J. H. & Jelínek E. 2006b: The Spačice eclogite: Constraints on the P-T-t history of the Gföhl granulite terrane, Moldanubian Zone, Bohemian Massif. Miner. Petrology 86, 203-220.

Messiga B. & Bettini E. 1990: Reactions behaviour during kelyphite and symplectite formation: a case study of mafic granulites and eclogites from the Bohemian Massif. Eur. J. Mineral. 2, 125-144.

Méres Š. 2008: Garnets — important information resource about source area and parental rocks of the siliciclastic sedimentary rocks. In: Jurkovič Ľ. (Ed.): Conference "Cambelove dni 2008". Abstract Book, Comenius Univ., Bratislava, 37-43 (in Slovak with English abstract).

Méres Š. & Hovorka D. 1989: Metamorphic development of gneisses in the Suchý, Malá Magura and Malá Fatra Mts. (Central Slovakia). Miner. Slovaca 21, 3, 203-216 (in Slovak with English summary).

Méres Š. & Hovorka D. 1991: Geochemistry and metamorphic evolution of the Kohút crystalline complex mica schists (the Western Carpathians). Acta Geol. Geogr. Univ. Com. Geol. 47, 15-66.

Méres Š., Ivan P. & Hovorka D. 2000: Garnet-pyroxene metabasites and antigorite serpentinites — evidence of the leptyno-amphibolite complex in the Branisko Mts. (Tatric Unit, Central Western Carpathians). Miner. Slovaca 32, 479-486 (in Slovak with English summary).

Michalík J. 1994: Notes on the Paleogeography and Paleotectonics of the Western Carpathian area during the Mesozoic. Mitt. Öster. Geol. Gessell. 86, 101-110.

Mikuš T. 2005: Cr-spinels from the Mesozoic sequences of the Western Carpathians. Phd Thesis, SAS, Bratislava, 1-110.

Mikuš T. & Spišiak J. 2007: Chemical composition and alteration of Crspinels from Meliata and Penninic serpentinized peridotites (Western Carpathians and Eastern Alps). Geol. Quart. 51, 257-270.

Mišík M. 1978: Some paleogeographic problems of the Pieniny Klippen Belt. In: Vozár J. (Ed.): Paleogeographic development of the Western Carpathians. GÚDŠ, Bratislava, 147-159 (in Slovak).

Mišík M. 1996: About the sedimentary area of the Klape Unit. Miner. Slovaca 28, 73-75 (in Slovak).

Mišík M. & Sýkora M. 1981: Pieniny exotic ridge reconstructed from pebbles of carbonate rocks of Cretaceous conglomerates of the Pieniny Klippen Belt and Manín Unit. Západ. Karpaty, Sér. Geol. 7, 7-111 (in Slovak with English summary).

Mišík M., Jablonský J., Fejdi P. & Sýkora M. 1980: Chromian and ferrian spinels from Cretaceous sediments of the West Carpathians. Miner. Slovaca 12, 209-228.

Mišík M., Jablonský J., Fejdi P. & Sýkora M. 1981: Spinels from Cretaceous sediments of the Western Carpathians. Folia Fac. Sci. Nat. Univ. Purk. Brun. 22, Geologia 3, 95-99 (in Slovak).

Mišík M., Mock R. & Sýkora M. 1977: Die Trias der Klippenzone der Karpaten. Geol. Zbor. Geol. Carpath. 28, 27-70.

Mock R., Sýkora M., Aubrecht R., Ožvoldová L., Kronome B., Reichwalder P. & Jablonský J. 1998: Petrology and stratigraphy of the Meliaticum near the Meliata and Jaklovce Villages, Slovakia. Slovak Geol. Mag. 4, 223-260.

Nakamura D., Svojtka M., Naemura K. & Hirajima T. 2004: Very high-pressure (> 4 GPa) eclogite associated with the Moldanubian Zone garnet peridotite (Nové Dvory, Czech Republic). J. Metamorph. Geology 22, 593-603.

Oberc J. 1972: Geological structure of Poland. Tectonics 2. Wydaw. Geol., Warszawa, 1-307 (in Polish).

O'Brien P. J. & Vrána S. 1995: Eclogites with a short-lived granulite facies overprint in the Moldanubian Zone, Czech Republic: petrology, geochemistry and diffusion modeling of garnet zoning. Geol. Rdsch. 84, 473-488.

O'Brien P. J., Kröner A., Jaeckel P., Hegner E., Żelaźniewicz A. & Kryza R. 1997: Petrological and isotopic studies on Paleozoic high-pressure granulites, Góry Sowie Mts, Polish Sudetes. J. Petrology 38, 433-456.

Oszczypko N. & Salata D. 2005: Provenance analyses of the Late Cretaceous-Palaeocene deposits of the Magura Basin (Polish Western Carpathians) — evidence from a study of the heavy minerals. Acta Geol. Pol. 55, 237-267.

Otava J. & Sulovský P. 1998: Detrital garnets and chromites from the Ksiaz Formation, Swiebodzice Depression: implications for the Variscan evolution of Sudetes. Geolines 6, 49-50.

Otava J., Krejčí O. & Sulovský P. 1997: The first results of study of garnet chemistry from the sandstones of the Rača Unit of the Magura Flysch. Geol. Výzk. Mor. Slez. 1996, 39-42 (in Czech).

Otava J., Sulovský P. & Krejčí O. 1998: The results of chemistry of detrital garnets from the Cretaceous sediments of the Rača Unit, Magura Group. Geol. Výzk. Mor. Slez. 1997, 1012 (in Czech).

Otava J., Sulovský P. & Čopjaková R. 2000: Changes in provenance of greywackes from the Drahany Culm Basin: statistical evaluation. Geol. Výzk. Mor. Slez. 1999, 94-98 (in Czech).

Paszkowski M., Jachowicz M., Michalik M., Teller L., Uchman A. & Urbanek Z. 1995: Composition, age and provenance of gravelsized clasts from the Upper Carboniferous of the Upper Silesia Coal Basin (Poland). Stud. Geol. Pol. 108, 45-127.

Plašienka D. 1995: Mesozoic evolution of Tatric units in the Malé Karpaty and Považský Inovec Mts: Implications for the position of the Klape and related units in Western Slovakia. Geol. Carpathica 46, 101-112.

Plašienka D. 1996: Cryptic ridges or collisional belts? Miner. Slovaca 28, 75-79 (in Slovak with English summary).

Pober E. & Faupl P. 1988: The chemistry of detrital chromian spinels and its implications for the geodynamic evolution of the Eastern Alps. Geol. Rdsch. 77, 641-670.

Racek M., Štípská P. & Powell R. 2008: Garnet-clinopyroxene intermediate granulites in the St. Leonhard massif of the Bohemian Massif: ultrahigh-temperature metamorphism at high pressure or not? J. Metamorph. Geology 26, 253-271.

Rybár A. & Kantor J. 1978: Radiometric dating of selected formation of the Western Carpathians 40Ar/40K age of the eruptives from Upohlav Conglomerates of the Pieniny Klippen Belt. Unpubl. Manuscript, Geofond archive, Bratislava, 1-67 (in Slovak).

Salata D. 2004: Detrital garnets from the Upper Cretaceous-Paleogene sandstones of the Polish part of the Magura Nappe and the Pieniny Klippen Belt: chemical constraints. Ann. Soc. Geol. Pol. 74, 351-364.

Samuel O., Borza K. & Köhler E. 1972: Microfauna and lithostratigraphy of the Paleogene and adjacent Cretaceous of the Middle Váh Valley (West Carpathians). GÚDŠ, Bratislava, 1-246.

Scharbert H. G. & Carswell D. A. 1983: Petrology of garnet-clinopyroxene rocks in a granulite-facies environment, Bohemian massif of Lower Austria. Bull. Miner. 106, 761-774.

Schulze D. J. 1997: The significance of eclogite and Cr-poor megacryst garnets in diamond exploration. Explor. Min. Geol. 6, 349-366.

Seifert A. V. & Vrána S. 2005: Bohemian garnet. Bull. Geosci. 80, 113-124.

Smulikowski K. 1967: Eclogites of the Śnießnik Mts. in the Sudetes. Geol. Sudet. 3, 7-180.

Šilar J. 1956: Occurrence of the Carboniferous coal in Senonian conglomerates in Váh valley near Púchov. Čas. Min. Geol. 1, 334-343 (in Czech with German summary).

Tomaś A., Olszewska B., Golonka J., Cieszkowski M. & Krobicki M. 2004: Devonian exotics in the Pieniny Klippen Belt flysch and their significance for the Paleozoic plate tectonic reconstruction of the West Carpathians. Geolines 17, 93-94.

Túnyi I. & Márton E. 2002: Cenozoic paleomagnetic rotations in the Inner Western Carpathians. Geol. Carpathica, Spec. Issue 53, 128-129.

Uher P. & Broska I. 1996: Post-orogenic Permian granitic rocks in the Western Carpathian-Pannonian area: geochemistry, mineralogy and evolution. Geol. Carpathica 47, 311-321.

Uher P. & Marschalko R. 1993: Typology, zoning and chemistry of zircon from main types of granitic and rhyolitic pebbles in conglomerates of the Pieniny Klippen Belt Cretaceous Flysch (Western Slovak segment, Western Carpathians). Geol. Carpathica 45, 171-184.

Uher P. & Pushkarev Yu. 1994: Granitic pebbles of the Cretaceous flysch of the Pieniny Klippen Belt, Western Carpathians: U/Pb zircon ages. Geol. Carpathica 45, 375-378.

Uher P., Marschalko R., Martini E., Puškelová Ľ., Streško V., Toman B. & Walzel E. 1994: Geochemical characterization of granitic rocks pebbles from Cretaceous-Paleogene flysch of the Pieniny Klippen Belt. Geol. Carpathica 44, 113-122.

Vozárová A. & Faryad S. W. 1997: Petrology of Branisko crystalline rock complex. In: Grecula P., Hovorka D. & Putiš M. (Eds.): Geological evolution of the Western Carpathians. Miner. Slovaca — Monograph., Bratislava, 343-350.

Vrána V., Štědrá V. & Fišera M. 2005: Petrology and geochemistry of the Běstvina granulite body metamorphosed at eclogite facies conditions, Bohemian Massif. J. Czech Geol. Soc. 50, 95-106.

Wagreich M., Faupl P. & Schlagintweit F. 1995: Heavy minerals from Urgonian Limestone pebbles of the Northern Calcareous Alps (Austria, Bavaria): further evidence for an intra-Austroalpine suture zone. Geol. Carpathica 46, 197-204.

Wierzbowski A., Aubrecht R., Krobicki M., Matyja B. A. & Schlögl J. 2004: New data on Jurassic stratigraphy and palaeogeography of the Czertezik Succession, Pieniny Klippen Belt (Western Carpathians) of Poland and Slovakia. Ann. Soc. Geol. Pol. 74, 3, 237-256.

Wieser T. 1985: Some remarks on the sedimentation, composition and provenance of exotics-bearing conglomerates in the Western Polish Carpathians flysch formations. In: Wieser T. (Ed.): Fundamental researches in the western part of the Polish Carpathians. Guide to excursion 1. XIII CBGA Congress, Cracow, Poland, 57-68.

Zoubek V. 1931: Caractéristique de quelques roches cristallophylliennes et éruptives des galěts exotiques des conglomérats sénoniens et paléog nes des Carpathes occidentales. Knih. St. Geol. Úst. ČSR 13, 353-358.

Geologica Carpathica

The Journal of Geological Institute of Slovak Academy of Sciences

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